Article:
Basal Balinka Conglomerates in the southern part of the Boskovice Basin between Moravský Krumlov and Veverská Bítýška: correlation lithostratigraphic horizon? (2024/2)Hršelová, P., † Houzar, S., Buriánek, D., Štelcl, J., 2024: Bazální balinské slepence v jižní části boskovické pánve mezi Moravským Krumlovem a Veverskou Bítýškou: korelační litostratigrafický horizont? – Acta Mus. Morav., Sci. Geol., 109, 2, 213–233 (with English summary).
Upper Carboniferous Balinka conglomerates were deposited along the western limb of the Boskovice Basin (eastern part of the Bohemian Massif). They may be locally developed as breccias along its base, tran sitioning into predominant conglomerates and passing gradually into the overlying medium- to fine-grained…
Article PDFArticle:
Green chromium-bearing mica in Balinka Conglomerates of Rosice-Oslavany Formation (Upper Carboniferous) at Oslavany (2013/1)Houzar, S., Kopečná, P., Štelcl, J., Vávra, , V., 2013: Zelená slída s podílem chromu v balinských slepencích rosicko-oslavanského souvrství (svrchní karbon) u Oslavan. – Acta Mus. Morav., Sci. Geol., 98, 1, 3–12 (with English summary)
Green chromium-bearing mica in Balinka Conglomerates of Rosice-Oslavany Formation (Upper Carboniferous) at Oslavany
Clasts of light-green mica containing chromium were recorded in the Upper Carboniferous conglomerates at Oslavany (Rosice-Oslavany Coalfield, Boskovice Graben). It is a potassium-deficient…
Article PDF
